Elliot Formation Stratigraphic range: Upper Triassic Lower Jurassic |
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Type | Geological formation |
The Elliot Formation is a geological formation dating to roughly 210 to 190 million years ago and covering the Norian to Sinemurian stages. The Elliot Formation is found in South Africa and Lesotho and is a member of the Stormberg Group. It consists mainly of limestone, sandstone, and mudstone. Fossils of the prosauropod dinosaur Massospondylus have been recovered from the upper Elliot Formation.
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Unidentified dinosaur eggs have been recovered from the formation.[2]
An unnamed ornithischian genus has been reported from the Upper Elliot Formation.[2] Geographically it was located in the Mafeteng district, Lesotho.[2] Ornithischian tracks have been reported from the Upper Elliot Formation.[2] Geographically they were located in Leribe District,[1], Mafeteng district, and Mohales Hoek District, Lesotho.[2] Possible indeterminate ornithischian remains have been reported from the Lower and Upper Elliot Formation of Cape Province, South Africa[1] and the Mohales Hoek District, Lesotho.[2]
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Notes Uncertain or tentative data are in small text; |
Ornithischian dinosaurs of the Elliot Formation | ||||||
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Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
A. consors[2] |
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"[Two] skulls, [one] associated with fragmentary skeleton; material consisting of either male and female or adult and juvenile."[3] |
The Qacha's Nek District remains were once considered Lycorhinus consors.[2] |
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F. australis[2] |
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"Fragmentary dentary with teeth."[4] |
Its remains are now considered indeterminate ornithischian.[2] |
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H. tucki[2] |
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Indeterminate[2] |
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L. scalpridens |
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Now regarded as a junior synonym of Lycorhinus. |
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L. diagnosticus[1] |
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"At least [four] skulls and associated skeletal material."[5] |
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L. angustidens[2] |
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"Isolated dentary maxillae."[3] |
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L. consors[2] |
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Split off as the type species of the new genus Abrictosaurus. |
Prosauropod tracks have been found in the Lower and Upper Elliot Formation.[1][2] Geographically, these finds have been located in Leribe District, Mafeteng District, Mohales Hoek district, Quthing District,[2] and Maseru District, Lesotho.[1] Possible prosauropod tracks have been located in the Lower Elliot Formation. Geographically these were located in Cape Province, South Africa.[1]
Color key
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Notes Uncertain or tentative data are in small text; |
Sauropodomorph dinosaurs of the Elliot Formation | ||||||
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Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
A. celestae |
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A. palustris |
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"Cervicals, caudals, partial fore- and hindlimb."[6] |
Elliot material formerly referred to this taxon was later concluded to be indeterminate prosauropod remains.[2] |
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A. ingenipes[1] |
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B. cromptoni[1] |
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"Associated left tibia, fibula, tarsus, [and] pes."[7] |
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D. gracilis |
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Elliot material formerly referred to this taxon was later concluded to be indeterminate prosauropod remains.[2] |
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E. fortis |
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"Fragmentary skeleton."[6] |
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E. africanus |
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"Vertebrae, ischia, incomplete ilia, tibiae and femora."[6] |
Elliot material formerly referred to this taxon was later concluded to be indeterminate prosauropod remains.[1] |
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E. browni[1] |
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Indeterminate[1] |
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G. africanus |
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"Vertebrae, both manus, pelvis and hindlimbs."[6] |
A valid sauropodomorph genus and species.[8] |
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G. taylori |
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"Sacrals, pelvic girdle."[6] |
Elliot material formerly referred to this taxon was later concluded to be indeterminate prosauropod remains.[2] |
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Indeterminate[2] |
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H. skirtopodus |
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Elliot material formerly referred to this taxon was later concluded to be indeterminate prosauropod remains.[2] |
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I. rachelis[9] |
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L. capensis |
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"Caudals."[6] |
Elliot material formerly referred to this taxon was later concluded to be indeterminate prosauropod remains.[2] |
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M. browni |
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"Cervicals, dorsal, caudals, pedal elements."[6] |
Elliot material formerly referred to this taxon was later concluded to be indeterminate prosauropod remains.[2] |
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M. carinatus[2] |
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M. harriesi |
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"Forelimb."[6] |
Elliot material formerly referred to this taxon was later concluded to be indeterminate prosauropod remains.[2] |
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M. schwarzi |
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Elliot material formerly referred to this taxon was later concluded to be indeterminate prosauropod remains.[2] |
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Indeterminate[2] |
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M. readi[1] |
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"[Three] partial skeletons, adult."[10] |
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M. thabanensis[2] |
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"Femur, adult."[10] |
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Indeterminate[1] |
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O. capensis |
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"Proximal tibia."[6] |
Elliot material formerly referred to this taxon was later concluded to be indeterminate prosauropod remains.[1] |
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P. orpenii |
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"Fragmentary vertebrae."[6] |
Elliot material formerly referred to this taxon was later concluded to be indeterminate prosauropod remains.[2] |
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P. cullingworthi |
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"Partial skeleton."[6] |
Elliot material formerly referred to this taxon was later concluded to be indeterminate prosauropod remains.[1] |
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P. stormbergensis |
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Elliot material formerly referred to this taxon was later concluded to be indeterminate prosauropod remains.[1] |
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T. browni |
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Elliot material formerly referred to this taxon was later concluded to be indeterminate prosauropod remains.[2] |
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T. minor |
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Elliot material formerly referred to this taxon was later concluded to be indeterminate prosauropod remains.[2] |
Theropod tracks are stratigraphically located in both the Lower and Upper Elliot Formation. Geographically, they are located in the Leribe District, Mafeteng District, Quthing District,[2] Maseru District and Mohales Hoek district,[1][2] Lesotho.[1]
Color key
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Notes Uncertain or tentative data are in small text; |
Theropod dinosaurs of the Elliot Formation | ||||||
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Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
A. rex[1] |
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Partial femur and possible maxilla.[11] |
Now known to be a chimera of Eucnemesaurus and a theropod mandible. |
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M. rhodesiensis[2] |
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S. rhodesiensis[2] |
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